In a companion paper concerning oceanic internal wave interactions (Lvov and Polzin, part I) we present two parallel derivations of spectral transport equations in an extreme scale separated limit; one based upon traditional wave turbulence theory techniques and one based upon ray tracing and path integral techniques. Both are generalized diffusion (Fokker-Planck) equations. However, they differ in that the ray-tracing version contains an explicit mean drift term. Evaluation of the extreme scale separated transports for the vertical wavenumber - vertical wavenumber component of the diffusivity tensor in the rotating limit leads to an immediate contradiction. The kinetic equation predicts no transport. The ray tracing transport equation returns a downscale transport that is an order of magnitude larger than metrics of ocean mixing known as 'Finescale Parameterizations' [1]}! The difference between these theoretical predictions and what is required by our observational knowledge of sources and sinks is such that we [2]}, [3]} refer to this growing set of contradictions as the 'Oceanic Ultraviolet Catastrophe'.
